Feldspars from pegmatites of Ravne in Carinthia

Authors

  • Ernest Faninger

Abstract

Feldspars of the Ravne pegmatites are composed of microcline, transitional varieties from orthoclase to microcline, and plagioclases showing characteristics from albite to oligoclase having 9 ½ percent anorthite on the average. The origin of the Ravne pegmatites is explained by the mobilization during a regional metamorphism. Their age is admitted to be Variscan.

Downloads

How to Cite

Faninger, E. (1981). Feldspars from pegmatites of Ravne in Carinthia. Geologija, 24(1), 75–87. Retrieved from https://www.geologija-revija.si/index.php/geologija/article/view/485

Issue

Section

Article